coasts Flashcards

(135 cards)

1
Q

what are sub aerial processes

A

include weathering and mass movement. These processes operate on the cliff face to weaken it and provide material for coastal erosion

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2
Q

what is the litteral zone

A

the coastal zone in which sediments are moved around between the land beach and sea

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3
Q

what is dynamic equilibrium

A

A systems inputs, process and outputs change but overall remain in a state of balance

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4
Q

why does the littoral zone constantly change (in the long and short term)

A

because of the dynamic interaction between the processes operating in the seas, oceans and on land
eg short term- due to individual waves, daily tides or seasonal changes
eg long term- due to the sea level changes or climate change

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5
Q

what are the sections of the littoral zone

A

backshore, foreshore (where most human activity occurs and where physical deposition, transport and mass movement largely occur) nearshore and offshore

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6
Q

what is the backshore zone affected by

A

only affected by waves during major storms and spring tides, normally high tides do not normally affect the backshore

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7
Q

what’s in the near shore

A

shallow waters nearest the land, also known as the breaker zone.

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8
Q

what part is the foreshore between

A

the part of a shore between high-tide and low-tide water marks. Also known as the surf zone.

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9
Q

under normal systems the coastal system operates in what state

A

dynamic equilibrium

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10
Q

what 4 factors are the dynamic equilibrium affected by

A
  • the sand supply (gives shoreline protection from the waves no sand= higher erosion rate)
  • the sea level
  • the waves (causes erosion most when wave is high)
  • the location of the shoreline (they more back and forth between storms and their location can either increase or decrease erosion rates)
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11
Q

what are the inputs of a coastal system (4)

A
  • marine- waves, tides,storm surges
  • atmospheric- weather/ climate, climate change
  • land- rock type/ structure, tectonic activity
  • people- human activity, coastal management
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12
Q

what are the processes of a coastal system (5)

A
  • weathering
  • mass movement
  • erosion
  • transport
  • deposition
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13
Q

what are the outputs of a coastal system

A
  • erosional landforms
  • depositional landforms
  • different types of coasts
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14
Q

how can coasts be classified (energy, geology) (6)
what does the land look like there

A
  • low energy- rate of deposition exceeds rate of erosion
  • high energy- rate of erosion exceeds rate of deposition
  • discordant- alternative layers of hard and soft rock perpendicular to the sea
  • concordant- alternative layers of hard and soft rock parallel to the sea
  • emergent
  • submergent
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15
Q

what is an emergent coast
and eustatic and isostatic change

A
  • land rising faster than sea level rises globally
  • eustatic change-change in sea levels due to glacial melt and the volume of water or tectonic activity change the shape of basins
  • isostatic change- crust changes height locally due to tectonic or less weight from glaciers (as they melt)
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16
Q

what is a submergent coast

A

flooded due to sea level rise globally
land sinking locally

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17
Q

rocky coasts result from …

A

(high and low relief) geology which is resistant to erosive forces of sea, rain and wind in a high energy environment

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18
Q

coastal plains are …

A

low-lying, low relief
result from supply of sediment from different terrestrial and offshore sources often in low energy environment

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19
Q

what is a cliff profile

A

the height and angle of a cliff face as well as its features eg wave cut platforms

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20
Q

what are features caused by erosion

A

headlands,bays,wave-cut notches and platforms, cave, arch, stack, stump

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21
Q

depositional coast features

A

beach, spit, bar, tombolo

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22
Q

what are the characteristics in lithology (geological structure) (6)

A
  • strata
  • bedding planes
  • joints
  • folds
  • faults
  • dip
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23
Q

what is a strata

A

is a layer of sedimentary rock or soil, or igneous rock that was formed at the Earth’s surface, with internally consistent characteristics that distinguish it from other layers.

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24
Q

what is a bedding plane

A

are formed due to longer or shorter pauses in the deposition process

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25
what is a joint
a fracture dividing rock into two sections that moved away from each other.
26
what is a fold
occurs when a stack of originally flat surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation
27
what is a fault
a crack in the Earth's crust. Typically, faults are associated with, or form, the boundaries between Earth's tectonic plates.
28
what is a dip
the acute angle that a rock surface makes with a horizontal plane
29
what is wave refraction And what are the waves like in a bay
is the bending of a wave as it spreads over different depths, shallow water depths usually slow down the wave and the height increases In bays, wave crests curve to fill the bay and wave height decreases
30
what is coastal recession
the retreat of a coastline due to erosion, sea-level rise or submergence
31
what is an igneous rock
erodes very slow have very few joints so there are limited weaknesses that erosion can exploit
32
what is a metamorphic rock
erodes slow are often folded and heavily fractured which are weaknesses that increase erosion
33
what is sedimentary rock
erodes fast young rocks tend to be weaker with more bedding places and fractures more vulnerable to erosion
34
what plants are good for stabilising sandy coastlines
xerophytes (found in sand dunes)- can tolerate very dry conditions halophytes (can tolerate salt water) marram grass sea couch
35
what is a sand dune
are small ridges of sand found at the top of a beach, form from wind blown sand that is initially deposited against an obstruction. vegetation binds the sand together and stabilises the dunes
36
what is a pioneer species
The first plants to grow in harsh coastal environments, paves way for other plants less able to survive in the conditions.
37
how are marshes formed
Flooded and drained by salt water brought in by the tides. the soil may be composed of deep mud and peat. peat is made up of decomposing plant matter that is often several feet thick and is waterlogged
38
what are mangrove forset ecosystems
Found in tropical locations along warm, shallow coasts. They are effective at reducing wave energy from tropical storms, cyclones, tsunamis. They are a natural coastal buffer to erosion and flooding
39
what factors affect coastal erosion rates
mangroves protect from erosion biological weathering with limited faults= more dfficult to erode deformation
40
what are waves
are a medium through which energy is transferred They are created by the wind blowing across the surface of the sea. Frictional drag increases as the wind speed increases, making the wave bigger.
41
what is the fetch
the distance a wave travels the maximum fetch is the distance from one coastline to the next landmass
42
why are beach profiles steeper in summer
when constructive waves are more common than destructive the swash of a constructive wave deposits larger material at the top of a beach creating a berm as it builds up the backwash becomes weaker.
43
why are beaches flatter in winter
berms are eroded by plunging waves and high-energy swash strong backwash transports sediment offshore
44
what are the erosion processes
hydraulic action, corrosion, abrasion, attrition
45
what is hydraulic action
Air trapped in cracks and fissures is compressed by the force of waves crashing against the cliff face. Pressure forces cracks open, meaning more air is trapped and greater force experienced in the next cycle of compression.
46
what is corrosion | (solution)
Carbonate rocks (limestones) are vulnerable to solution by rainwater, spray from the sea and seawater.
47
what is abrasion
Sediment picked up by breaking waves is thrown against the cliff face. The sediment acts like a tool on the cliff, chiselling away at the surface and gradually wearing it down by removing small rock particles.
48
what is attrition
This process acts on already eroded sediment. As sediment is moved around by waves, the numerous collisions between particles slowly chip fragments off the sediment.
49
what are the erosional processes influenced by
wave type and size and lithology
50
whihc factors erode coast more
* hydraulic action and abrasion are most dominant * the lithology bands of more resistant rock between weaker joins and cracks erode more slowly. This selective erosion is known as differential erosion.
51
what landforms can erosion make
wave cut notches, wave cut platforms, cliffs, the cave-arch-stack stump sequence
52
what is the process of a wave cut notch
eroded at the base of a cliff by hydraulic action and abrasion, as the notch becomes deeper, the overhanging rock above becomes unstable and eventually collapses as a rockfall. repeated cycles of notch cutting and collapse cause cliffs to reduce inland
53
what is a wave cut platform and its characteristics
the former cliff position after wave cut notches occur and is horizontal rock platform Slopes gently down to the angle of 3-4 degrees. An overall pitted appearance of bare rock interspersed with rock pools. Bare rock, smoothed in places by abrasion. Deep cracks in some places. Covered at high tide and exposed at low tides.
54
how does a wave cut platform form?
1.Destructive waves erode the cliff through processes such as abrasion and hydraulic action 2.Waves erode the cliff between the high and low tide lines. 3.Over time, this erosion creates a wave cut notch at the base of the cliff. 4.This notch gradually gets larger. The cliff above the wave cut notch is now unsupported 5.Mass movement (falling of material) occurs as a result of gravity and the cliff retreats. 6.The wave cut platform is the uneroded section of the original cliff at the base. 7.the process repeats and cliff continues retreating
55
what are the ways of sediment being transported along a coastline
traction, saltation, suspension, solution
56
what is traction
bigger pebbles and boulders are rolled along the sea bed
57
what is saltation
small pebbles moved when one pebble hits another, making it bounce. This bouncing sets up a chain reaction
58
what is suspension
fine sediment is carried as suspension in the water, this is what makes water look dirty.
59
what is solution
dissolved material is carried along and you can’t see it. (invisible)
60
how does longshore drift move sediment
the swash moves beach sediment up the beach at the same angle as wave approaches. the backwash of wach wave then carries the same sediments back down the beach at right angles to the shore
61
what is drift-aligned
wave crests break at an angle to the coast, so there is consistent longshore drift
62
what is swash-aligned
wave crests approach parallel to the coast, so there is limited longshore movement of sediment.
63
what is flocculation
is a depositional process that is important for very small particles, such as clay, which are so small they remain suspended in water. Clay particles clump together due to electrical or chemical attraction and become large enough to sink.
64
what is gravity settling
occurs when the energy of transporting water becomes too low to move sediment; large sediment will be deposited first
65
what are depositional landforms
beaches, recurved and double spits, offshore bars, barrier beaches and bars, tombolos and cuspate forelands
66
how is a storm beach formed and beach cusps
* Storm beaches are a ridge of boulders and shingle found at the back of a beach They result from high energy deposition at high tides or during severe storms. They are found on the backshore * Beach cusps are crescent shaped indentations that form on beaches of mixed sand and shingle- located in low energy bays
67
formation of a spit
sand or shingle is moved along the coast by longshore drift,but if the coastline suddenly changes direction then sediment will begin to be deposited and built up. the outward flow of the river will prevent the spit from extending the full width of the estuary. behind the spit a lagoon forms and sediment is deposited there and eventually builds up to sea level to form a salt marsh
68
how is a recurved spit formed
occasionally a storm comes in and causes the direction of the prevailing wind to change and moves sediment in a different direction forming the curve or hook when wind direction returns to normal the spit resumes its growth.
69
what is a double spit
formed from a breach of a pre existing spit or bar usually by a river or storm
70
what is a barrier beach (bar)
form in the same way as a spit initially but bars are created where a spit grows across a bay, joining two headlands. Behind the bar, a lagoon is created, where water has been trapped and the lagoon may gradually be infilled as a salt marsh develops due to it being a low energy zone, which encourages deposition.
71
what is a barrier island
These can be formed by rising sea level when a barrier beach becomes separated from the mainland forming a ridge or island.
72
how is an offshore bar formed
also known as sandbars are submerged or partly exposed ridges or coarse sediment. They are created by waves that operate offshore from the coast. destructive waves erode sand from beach and swash which removes sediment and deposits it offshore as bars
73
how is a tombolo formed
a beach formed between a small island and the mainland and deposition occurs where waves lose energy and tombolo builds up * Waves are refracted around the island & set up 2 opposing LSD directions. * These merge behind the island & sand is deposited linking the mainland & the island
74
how are cuspate forlands formed
is a triangular-shaped headland that extends from main coastline * They form where the coast is exposed to longshore drift from opposite directions * Sediment is deposited at the point where they meet and forms a natural triangular shape * Vegetation eventually grows and stabilises the sediment.
75
what are the types of weathering (3)
mechanical, chemical, biological
76
what is weathering
is the breaking down of rock into smaller particles. Weathering processes include freeze thaw action, acid rain dissolution, root growth, heat expansion cracking
77
what is subaerial
occuring or formed in the open air include weathering and mass movement. operate on the cliff face to weaken it and provide material for coastal erosion
78
what is mechanical weathering
* caused by physical changes such as changes in temperature, freezing and thawing, and the effects of wind, rain and waves.
79
how does mechanical temp changes cause weathering
temperture- When a rock gets hot it expands a little, and when a rock gets cold it contracts a little. If a rock is heated and cooled many times, cracks form and rocks fall away
80
how does mechanical freeze-thaw cause weathering
Water expands slightly when it freezes into ice. so as it gets into cracks in rocks and freezes it causes crack to expand and rock breaks off
81
what is salt crystalisation and wet and drying cause weathering
* when salt crystals are deposited in cracks and over time the salt accumulates and applies pressure to the crack * wet rocks may expand (clay) and contract when dry causes cracks and vulnerable to freeze thaw and salt crystalisation
82
what is biological weathering and root boring
speeds up mechanical and chemical weathering throught the action of plants, bacteria or animals root boring occurs when clams and molluscs bore into rock and may also secrete chemicals that dissolve rocks
83
what is chemical weathering and carbonation+ hydrolysis+ oxidation
* involves decomposition of rocks changing the minerals occurs as a result of a weak chemical reaction between water and rock * Rainwater mixed with carbon dioxide in the atmosphere forms Carbonic acid. This then reacts with calcium carbonate in limestone to form calcium bicarbonate. Bicarbonate is soluble in water and the limestone gets weathered when carbonation occurs. * The breakdown of minerals to form new clay minerals plus materials in solution * The addition of oxygen to minerals which produces iron oxides and increases volume which contributes to mechanical breakdown.
84
what is mass movement and the types (5)
the down slope movement of earth materials under gravity 1. rock falls 2. translational slides 3. rotational slumping 4. topples 5. flows
85
when is rock fall likely to occur
when strong jointed and steep rock faces are exposed to mechanical weathering. Occur on slopes over 40 degrees. the material either bounces or falls vertically to form scree
86
what is a translational slide
rocks that are jointed or have bedding planes roughly parallel to the slope or cliff surface are susceptible to landslides. an increase in the amount of water can reduce friction- causing sliding in a rock or landslide, slabs or blocks can slide underlying rocks along a slipe plane or slide.
87
when do rotational slide/slump occur and what do they leave
in saturated conditions, slip on moderate to steep slopes common where softer materials overlie more resistant or impermeable rocks (limestone) causes rotational scars on the land and repeated slumping causes terraced cliff profiles they leave marks on the landscape known as rotational scars
88
when do topples occur
the is influenced by the geological structure of the rock face where rock strata have a steep seaward dip, undercutting by erosion will quickly lead to instability and blocks of material falling seawards
89
when does a flow occur
an increase in the amount of water can reduce friction and cause mud and earth to flow over the underlying bedrock the difference between a slide and a flow is that in a slide the material remains intact in a flow it becomes jumbled up.
90
what do repeated rotational slumping create
terraced cliff profile
91
sea level change can change in the short term
due to high and low tides Atmospheric air pressure (low pressure causes slight rise in sea level) Winds which can push water towards the coast and wave heights which vary
92
types of sea level change the land or the sea rises or falls (2)
eustatic change isostatic change
93
what is eustatic change
Global-scale sea level change caused by a change in the volume of water in the ocean store Heating of ocean water causes the water molecules to move, The free movement of these particles causes the expansion of liquid.
94
what is isostatic change
Local-scale sea level change caused by a change in the level of the land relative to the level of the sea.
95
what is emergence or submergence
emergent coasts- where the coasts are rising relative to sea level, for example due to tectonic uplift Submergent coasts – are being flooded by the sea, either due to rising sea levels and/or subsiding land
96
what is isostatic subsidence
When the weight of an ice sheet on land causes it to sink, this give the appearance that the sea has risen. | eg Scotland
97
what is isostatic recovery
When the ice melts the reduced weight causes the land to readjust and rise, this can give the appearance that the sea level is falling. | eg england+ wales
98
what factors do an emergent coast have
a raised beach- areas of former wave-cut platforms and their beaches left at a higher level than present sea level due to sea level change. They are found at a distance inland from the present coastline.
99
proof of land level rise emergence coasts (2)
raised beaches- little Gruinard (NW scotland) abandoned cliff line- Kings cave (have caves cut by marine erosion but are now left higher and dry + unaffected by marine erosion
100
proof of sea level rise submergence coasts (2)
Ria- are submerged river valleys- lowest part of the river's coarse and the floodplains may be completely drowned but tops of valley course remain exposed (Kingsbridge Ria- south devon) Fjord- are submerged glacial valleys- have very steep sides and the water in a fjord is very deep (Milford Sound- New Zealand) Barrier islands- formed initially as lines of coastal sand dunes attatched to the shore. sea level rise floods the land behind form a lagoon, leaving the dunes as islands (East coast of America) Dalmation coasts- form where there are hills running parallel to the coast. rising sea levels submerge the area to create long narrow islands arranged in lines. ( dalmation coast-Croatia) tectonic activity raised beaches- a series of storm beach ridges. The ridge very close to the shore is the present storm beach ridge. then there is previous inland ridges (New Zealand)
101
human and physical factors of coastal recession
human- dredging, dams or coastal management eg groynes physical- geological eg softer= vulnerable to mass movement weathering and erosion, marine eg long wave fetch, strong longshore drift erode debris quickly
102
holderness coast
* average it loses 2m of a coastline every year * lack of physical protection of cliffs by narrow and low beaches * has boulder clay that can easily be eroded
103
what impacts are there for coastal management
erosion rates increase further down variation in cliff height
104
what are ORDS
deep hollows on the beach which run parallel to teh cliff line- they concentrate erosion in particular locations by allowing the waves to directly hit the cliff with little energy dissipation on the beach they erode 4x faster than areas withour ORDS
105
what are economic reasons to inhabit the areas that are at risk from erosion and have the threat of flooding
* coastlines are popular with tourists, especially when access to beaches and the sea is easy * deltas and esuaries are ideal locations for trade * delatas are especially fertile and ideal for farming
106
increase in sea level rise
* sediment trapped by upstream dams, reduce new deposition on delta surface * sea level rise increases flood risk and erosion storm surges from hurricanes flood the delta more frequently * delta subsidence is caused by weight of sediment deposition, which balanced on the delta surfaces * destruction of mangrove forests for wood and charcoal exposes the coast to erosion * river straightening for navigation means faster river flow and sediment being propelled too far offshore
107
what is a storm surge
is a short-term change in sea level caused by low air pressure which can be a depression, or a tropical cyclone
108
what is a depression
low pressure weather system in the mid-latitides, eg uk
109
coastal flooding is made worse when (3)
* strong winds push waves onshore, so wave height increases * high or spring tide occur at the same time as the storm * sea bed shallowes towards the coast
110
when is the rise in sea level during a storm surge intensified
when the coastline is funnel-shaped and causes severe coastal flooding
111
what are human reasons for coastal risk and flooding (3)
* dams * urbanisation * deforestation
112
what are physical reasons for coastal risk and flooding (5)
* isostatic * eustatic * low lying delta * topography * cyclone/storm surge
113
how does climate change increase risk at the coast
* sea level rising * 50% increase in delta flooding * strorm surges linked to depressions will become more common * higher erosion
114
how can the effects of climate change be managed
adaptation- making changes to lessen the impact- include building sea walls, storm surge barriers, reinstating mangrove forests mitigation- making efforts to reduce the emissions of greenhouse gases- finding alternative renewable sources of energy, cleaner industry, hybrid/electric cars, housing insulation, turning off lights etc
115
consequences of coastal recession (causes, social and economic)
causes= Lithology; Geological structure; waves; human intervention. social=Impacts on people - costs of relocation; employment; businesses and agricultural land. Mental health - stress and worry linked to recession - Hard to quantify. Loss of amenity value. economic=Costs of; businesses and agricultural land. Repairs e.g. roads, trains.
116
consequences of coastal flooding (causes, social and economic)
causes=Cyclones; Storm surges; SL rise; urbanisation; deforestation (mangroves) social= Loss of homes; loss of life; people homeless. Stress and bereavement etc. economic= Loss of land; damage to homes and infrastructure. Economic losses (wages).
117
economic losses due to coastal erosion
loss of or damage to property in form of homes, businesses and farmland is easy to quantify in Uk gov dont provide compensation to people who lose their homes to coastal erosion
118
social losses due to coastal erosion
relocation break up of community loss of friends stressful source of income
119
what are environmental refugees
are those forced to leave their homes because of natural processes, including sudden ones such as landslides or gradual ones such as erosion or rising sea levels predicts sea level rise by 2100 would leave envir refugees due to flooding, salt water encroachment, coral bleaching
120
what is a mega project
a very expensive (over US$1 billion), technically difficult and usually long-term engineering project. Have multiple aims
121
what is a return period (or reccurence interval)
Refers to the frequency of a flood of a particular magnitude. A 1:100 flood event will occur, on average, every 100 years
122
how can prevent coastal erosion (3)
hard engineering- using artificial structures to defend land against natural erosion processes soft engineering- by working with natural processes to help restore beaches / ecosystems and reduce erosion. mitigation- to manage the coastal zone in terms of people’s economic/social/cultural well being as well as minimising environmental impacts. It encourages communities to adapt to the threats
123
what are examples of hard engineering on a coastline (5)
1. groynes 2. sea walls 3. rip rap 4. revetmentsz 5. offshore breakwaters
124
what are the advantages and disadvantages of groynes
ad- maintain the size of a beach protects coast at the point. enhance the beach enhance tourism less expensive than sea walls dis-expensive due to difficulties in getting firm foundations in a beach. may be an obstacle to people moving along a beach not natural so could be eyesoar greatly reduce longshore drift transport may cause narrower beaches and increased erosion down drift
125
advantage and disadvantages of sea walls
ad- made of long lasting concrete and able to absorb wave energy give people confidence and a sense of security the tops can be used as promenades dis- most expensive do not fit in with natural surroundings accessing beach may be difficult
126
what are advantages and disadvantages of rip rap
ad- long lasting and flexible to use placed at susceptible points on the backshore to protect base of sea wall or groyne dis- maylool unsightly can create difficult access as difficult to climb over seawater can move through it so some weathering and erosion may still occur ## Footnote (boulders concrete shapes)
127
what are advantages and disadvantages of revetments
ad- absorb wave energy trap beach sediment behind them longshore drift can continue cheaper to sea walls dis- reduce access to beach looks unsightly may need constant maintenance ## Footnote are sloped walls often made of wood
128
what are advantages and disadvantages of offshore breakwater
ad- proved effective create sheltered water areas behind them for water sports and tourism used to protect entrance to harbours dis- look unsightly may need olther coastal engineering create increased deposition on the landward side ## Footnote rock boulders (usually granite) dropped and aligned in short lengths in shallow nearshore waters parallel to the shore
129
what are soft engineering approaches to coastal erosion (4)
1. beach nourishment 2. cliff regrading (cut the cliff slope to a stable angle) 3. cliff drainage (when cliff lithology consists of a permeable layer above impermeable layer: drains with gravel can be inserted to drain water out fast) 4. dune stabilisation (replant grass)
130
what is sustainable coastal management
Managing the wider coastal zone in terms of people and their economic livelihoods, social and cultural well-being, and safety from coastal hazards, as well as minimising environmental and ecological impacts.
131
examples of sustainable coastal management (6)
* managing natural resources= long term productivity * managing flood and erosion risk/ relocating to safe areas * create alternative livelihoods before existing ones are lost * adapting to rising sea levels by relocating alternative building methods * educate communities * monitering coastal change and adapt to unexpected trend
132
ICZM means that (5)
coastal management must: * plan for the long term * involve all stakeholders * adopt ‘adaptive management’, changing plans and policies if threats change * try to work with natural processes, not against them * use ‘participatory planning’ where all stakeholders have a say in any policy decisions.
133
how many sediment cells are there and how are they managed
there are 11 is managed either as a whole unit or a sub-unit and a shoreline management plan (SMP) is used
134
what are the 4 policies that can be used on a shoreline management plan
1. hold the existing shoreline 2. advance the existing shoreline 3. managed realignment of the shoreline 4. no active intervention
135
what are the 4 policies that can be used on a shoreline management plan based on what complex judgements
engineering feasibility environmental sensitivity land value political and social reasons cost benefit analysis (CBA) environmental impact assessment (EIA)